Reactions of thiophene and methylthiophenes in the interlayer of transition-metal ion-exchanged montmorillonite studied by resonance Raman spectroscopy
Reactions of thiophene and methylthiophenes in the interlayer of transition-metal ion-exchanged montmorillonite studied by resonance Raman spectroscopy
Clays and Clay Minerals (February 1987) 35 (1): 53-59
- adsorption
- Asia
- bentonite
- clastic rocks
- clay mineralogy
- clay minerals
- crystal chemistry
- Far East
- geochemistry
- ion exchange
- Japan
- mineral data
- minerals
- montmorillonite
- organic compounds
- organic materials
- polymerization
- Raman spectra
- sedimentary rocks
- sheet silicates
- silicates
- spectra
- thiophene
- methylthiophenes
The adsorption and reaction of thiophene and methylthiophenes in the interlayer of Cu (super 2+) - and Fe (super 3+) -montmorillonites were investigated by resonance Raman spectroscopy. Thiophene and 3-methyl-thiophene polymerized to form cations of polythiophene and polymethylthiophene respectively, which were characterized by absorption bands in the near-infrared region. These polymer cations formed in the interlayer were reduced to their neutral polymers if the clay-polymer complexes were in contact with water, and the formation of their neutral polymers was clearly demonstrated by their resonance Raman spectra. 2,5-Dimethylthiophene in which polymerization was hindered by methyl substitution at the 2 and 5 positions, was oxidized to 2,5-dimethylthiophene cation in the interlayer.